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XIA Yubo, WANG Bing, LI Haitao, MA Zhen, GUO Xu, ZHAO Kai, ZHAO Changrong, ZHANG Xi, WANG Xiaoxu. 2025. Study on hydrochemical origins and health geology regionalization of shallow groundwater in Xiong'an New Area[J]. Geology in China, 52(1): 331-346. doi: 10.12029/gc20220323007
Citation: XIA Yubo, WANG Bing, LI Haitao, MA Zhen, GUO Xu, ZHAO Kai, ZHAO Changrong, ZHANG Xi, WANG Xiaoxu. 2025. Study on hydrochemical origins and health geology regionalization of shallow groundwater in Xiong'an New Area[J]. Geology in China, 52(1): 331-346. doi: 10.12029/gc20220323007
shu

Study on hydrochemical origins and health geology regionalization of shallow groundwater in Xiong'an New Area

  • 1.

    Tianjin Center (North China Center for Geoscience Innovation), China Geological Survey, Tianjin 300170, China

  • 2.

    Tianjin Key Laboratory of Coast Geological Processes and Environmental Safety, Tianjin 300170, China

  • 3.

    Xiong'an Urban Geological Research Center, China Geological Survey, Tianjin 300170, China

  • 4.

    Tianjin Geothermal Exploration and Development-Designing Institute, Tianjin 300250, China

  • 5.

    China Institute of Geo-Environment Monitoring, Beijing 100081, China

  • 6.

    BGI Engineering Consultants Ltd., Beijing 100038, China

  • 7.

    Planning and Construction Bureau of Xiong'an New Area, Xiong'an 071799, Hebei, China

    • Fund Project: Supported by the projects of China Geological Survey (No.DD20189122, No.DD20189142, No.DD20190338 and No.DD20221759).
More Information
  • Author Bio: XIA Yubo, male, born in 1982, professor level senior engineer, engaged in the survey and evaluation of urban geological, hydrogeology, engineering geology and environmental geology; E-mail: sosodragon@163.com
  • Corresponding author: LI Haitao, male, born in 1979, professor level senior engineer, engaged in hydrogeological and environmental geological survey, monitoring, evaluation and comprehensive research; E-mail: lihaitao@mail.cgs.gov.cn. 
Received Date:  23 March 2022
Revised Date:  19 May 2022
Publish Date:  25 January 2025
    Abstract

  • This paper is the result of hydrogeological survey engineering.

    Objective

    In hydrogeological contexts, biological growth and human health are closely linked to the concentrations of elements present in the surrounding environment, including water and soil. Investigating the formation and evolutionary conditions of both macro and trace elements associated with health in groundwater, as well as establishing regional health geology, is beneficial for advancing the implementation of the Healthy China strategy.

    Methods

    Xiong'an New Area was chosen as the primary research site. The hydrogeochemical characteristics and sources of mineral composition in shallow groundwater were analyzed using multivariate statistical analysis, as well as the Piper and Chadha diagrams. This study restored the water quality by identifying the material element sources of shallow groundwater along a typical profile, delineated hydrochemical types, and classified the differentiation areas of macro and trace elements based on biological necessity, environmental factors, and element abundance or deficiency. Furthermore, it established a health geology regionalization for Xiong'an New Area.

    Results

    The parameters of groundwater exhibited significant variability. The water−rock interactions indicate that the dissolution of albite contributes sodium ions (Na+), while the dissolution of fluorite and gypsum contributes fluoride ions (F−) and sulfate ions (SO42−), consuming calcium ions (Ca2+), magnesium ions (Mg2+), and bicarbonate ions (HCO3−), alongside the precipitation of calcite and dolomite, with reverse ion exchange also occurring. In the northern part of the study area, the predominant hydrochemical types were HCO3–Ca and HCO3–Ca·Mg. This composition transitioned to HCO3·SO4–Na·Mg·Ca, HCO3·Cl–Na·Ca·Mg, and HCO3·SO4·Cl–Na·Mg in the middle section, ultimately evolving into SO4·HCO3–Na·Mg in Baiyangdian and downstream of the Daqing River. Xiong'an New Area can be categorized into three regions: A health geology regionalization characterized by a deficiency of elements in the northern alluvial−proluvial plain; A health geology regionalization with moderate element levels in the interaction zone between the alluvial−proluvial plain and the alluvial−lacustrine plain; And a health geology regionalization with an excess of elements in the alluvial−lacustrine plain. Prolonged consumption of groundwater from both the deficient and excess areas may lead to health issues.

    Conclusions

    It is essential to examine the endemic diseases associated with the local surplus and deficiency of fluoride (F−), sulfate (SO42−), total hardness, and iodide (I−) in Xiong'an New Area. Additionally, identifying alternative water sources or supplementing the necessary elements for human health is crucial to support the Healthy China strategy.
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